Clarksville soil series
Loamy-skeletal, siliceous, semiactive, mesic Typic Paleudults
Ultisols — strongly weathered, leached soils with a clay-enriched subsoil
With 2.80 million acres mapped, Clarksville is the 17th-largest of 24,791 U.S. soil series. In Missouri only one series covers more ground. It dates from 1901; only four atlas series are older. Besides it, only Kalkaska and Troup are somewhat excessively drained in this atlas.
- Depth
- Very deep
- Drainage
- Somewhat excessively drained
- Water movement
- Moderately high
Where Clarksville is mapped
2,802,758 acres in 83 soil survey areas, from current SSURGO data.
How it is classified
- OrderUltisols
- SuborderUdults
- Great groupPaleudults
- SubgroupTypic Paleudults
- FamilyLoamy-skeletal, siliceous, semiactive, mesic Typic Paleudultsloamy-skeletal particle-size classsiliceous mineralogy classsemiactive cation-exchange activity classmesic soil temperature regime
Against other Ultisols
Clarksville makes up 1.48% of all mapped Ultisols — the 5th largest of 1,278 series in the order.
Solum thickness (topsoil + subsoil)
152 cm over a median of 142 cm
Depth to the subsoil
30 cm over a median of 23 cm
Depth described
152 cm under a median of 178 cm
Its relatives
Close relatives, at one scale
Horizon by horizon
| Horizon | Layer | Depth | Thickness |
|---|---|---|---|
| Oi | Organic layer: slightly decomposed | 0–3 cm0–1 in | 3 cm |
| A | Topsoil | 3–13 cm1–5 in | 10 cm |
| E | Leached layer | 13–30 cm5–12 in | 17 cm |
| Bt1 | Subsoil: clay build-up | 30–46 cm12–18 in | 16 cm |
| Bt2 | Subsoil: clay build-up | 46–74 cm18–29 in | 28 cm |
| 2Bt3 | Subsoil: clay build-up, different parent material | 74–104 cm29–41 in | 30 cm |
| 2Bt4 | Subsoil: clay build-up, different parent material | 104–132 cm41–52 in | 28 cm |
| 3Bt5 | Subsoil: clay build-up, different parent material | 132–152 cm52–60 in | 20 cm |
Sources: USDA–NRCS Official Series Description (revised 2004-06), Soil Classification database and SSURGO. Ranks computed by Soil Series Atlas. Method · Guides